1887
Volume 7 Number 4
  • E-ISSN: 1365-2478

Abstract

S

A uniform field of the normal geomagnetic vertical intensity and its normal dependence on the first and second powers of latitude and longitude are derived for Europe and represented by sketches. The epochs of 1938.5, 1941.5, 1944.5, 1947.5, 1950.5, 1953.5, and 1956.5 have been chosen.

It is suggested that anomalies of the vertical intensity should be given according to this field in order to obtain, in course of time, a coherent image of the magnetic effects of the European continent.

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/content/journals/10.1111/j.1365-2478.1959.tb01476.x
2006-04-27
2024-04-23
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http://instance.metastore.ingenta.com/content/journals/10.1111/j.1365-2478.1959.tb01476.x
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  • Article Type: Research Article

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